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Titan's methane likely comes from inside, not surface NASA-GODDARD NEWS RELEASE Posted: November 30, 2005 The methane giving an orange hue to Saturn's giant moon Titan likely comes from geologic processes in its interior according to measurements from the Gas Chromatograph Mass Spectrometer (GCMS), a Goddard Space Flight Center instrument aboard the European Space Agency's Huygens Probe. The GCMS, which descended with five other instruments on the probe through the moon's thick atmosphere on Jan. 14, 2005, also found evidence of liquid methane in the surface material.
The origin of methane in Titan's atmosphere is a mystery because it gets broken down by sunlight and particle radiation from space in the upper atmosphere. If surface lakes and pools were the only source, all of Titan's methane would be lost by this mechanism in less than a hundred million years, a short time for a moon that's been around since the formation of the solar system 4.5 billion years ago. Components of the methane molecules react with each other and atmospheric nitrogen. As they descend, they form larger and heavier molecules that comprise the orange haze that blankets the moon. Because Titan is very cold (292 degrees below zero F, or minus 180 degrees Celsius) these heavy compounds condense and rain out on the surface. "We have determined that Titan's methane is not of biological origin, so it must be replenished by geologic processes on Titan, perhaps venting from a supply in the interior that could have been trapped there as the moon formed," said Dr. Hasso Niemann of Goddard, principal investigator for the GCMS and lead author of a paper on this research to appear in Nature on Dec. 8.
The carbon in methane molecules comes in different varieties, or isotopes - carbon-12 (12C) and carbon-13 (13C). Each 13C atom has an extra neutron in its nucleus, making them slightly heavier than 12C atoms, so the GCMS can distinguish between methane with 12C and methane with 13C. Living organisms have a preference for carbon-12. As a result, carbon-containing molecules, such as methane, that are associated with life on Earth get enriched in 12C. The ratio of 12C to 13C is a marker or signature of life. However, the team did not see 12C enrichment in the methane on Titan. Also, when the heated inlet of the GCMS came in contact with the surface, it vaporized some of the surface material. After impact, the GCMS detected a 40 percent increase in the number of methane molecules measured, and this level remained for about 50 minutes after impact. This long-lived burst is best explained by the presence of liquid methane mixed with the surface material, according to the team. Other Huygens observations, such as pictures from the Descent Imager and Spectral Radiometer instrument, show features that look remarkably like dry riverbeds. Scientists have theorized that at Titan's cold temperatures, liquid methane plays the role of water on Earth, while deeply frozen water substitutes for rock. On Titan, liquid methane could cut channels in water ice the same way water carves canyons through rock. The presence of liquid methane on Titan's surface supports this scenario. The Cassini-Huygens mission is a cooperative project of NASA, ESA and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Cassini-Huygens mission for NASA's Science Mission Directorate, Washington, D.C. |
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VIDEO:
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